Development of a coastal prediction system that incorporates full three-dimensional wave-current interactions on the mean flow and the scalar transport with initial application to the Lake Michigan turbidity plume.

摘要

The present work focuses on the development of a Modular Multi-Component Coastal Ocean Prediction System (M2COPS) that incorporates the full 3D wave-current interactions for a better representation of the entrainment and transport mechanics in complex deep and shallow water coastal environments. The system incorporates wind, temperature and atmospheric pressure forcing that drive the circulation, wave, sediment and bottom boundary layer model components.;The effects of the wind generated surface waves on the water column and bottom layer dynamics are parametrized by the inclusion of the Stokes drift, and the wave radiation stress terms that quantify the excess of mass and momentum flux produced by the waves. Coupled wave-hydrodynamic models traditionally incorporate the radiation stress terms only into the vertically integrated momentum. Considering the fact that currents are 3D structures, the vertical variation of the radiation stress should be also considered. In the present work the 3D momentum equations are re-derived to include the full 3D impact of the radiation stresses on the currents.;As a preliminary test, the system is applied to Lake Michigan with a twofold purpose: (a) to conduct an initial testing of the model prognostic variables with and without the effect of the waves; and (b) to develop a methodology required to answer whether the annually observed Spring turbidity nearshore plume in Southern Lake Michigan is transporting material from its origin in one continuous transport mode or as generated by a series of local deposition, resuspension and transport activities. To this end data collected during the EEGLE project are fully analyzed; shoreline erosion rates and texture of the eroded material were collected from various sources and via various methods and are presented for 34 shoreline segments in a uniform format; an Eulerian Particle Tracking formulation that identifies the source and origin of the various particle sizes within the sediment plume is presented; and a conceptual and computational set up of the control volumes or sediment plume sources/origins required for a detailed study of the Spring turbidity plume is developed.